A kettle is a depression left by melted blocks of ice in glacial deposits.
Kettle holes are depressions left by melted blocks of ice in glacial deposits. These features are typically surrounded by mounds of sediment called kames. Kettle holes are common in areas that were once covered by glaciers during the last Ice Age.
The depressions left by melted blocks of ice in glacial deposits are called kettle holes. They are circular or oval-shaped depressions that form when large chunks of ice left behind by a retreating glacier become buried in sediment. When the ice eventually melts, it creates a hole in the ground.
The depressions left behind are called kettles. The raised areas are called moraines.
glacial lakes. These lakes were formed by the meltwater from the ice blocks, and often occupied depressions in the landscape created by glacial activity. They were temporary features that eventually drained as the ice melted away completely.
kettle
When the glacier melted from North America it left a mass of "heterogeneous" rock debris (loosely termed "glacial drift") etc
All over the world. They can be found anywhere from on a mountain, like at Mount Washington's Lake of the Clouds Hut, to underground, like at Howe's Caverns.
A moraine is a landscape feature created by glacial deposits. Moraines are formations of unsorted rock debris that were transported and deposited by a glacier as it moved and melted. They can be found in various forms such as terminal moraines at the end of glaciers or lateral moraines along their sides.
Glacial errosion
a glacial deposit that is sorted and layered by streams or melted water is called
A kettle pond is a shallow, sediment-filled body of water formed by retreating glaciers during the last ice age. They are typically small and round, and can be found in regions that were once covered by glaciers.
A cirque is a bowl-shaped depression formed by glacial erosion, typically found in mountainous regions. It often features steep sides and a flat floor, which can collect snow and ice. A tarn is a small mountain lake that forms in the basin of a cirque when the melted water accumulates. Thus, a cirque without a tarn would be a glacial depression that lacks this body of water, potentially dry or filled with sediment instead.